The underwater landslide, 75km off the Queensland Coast at a site now known as Gloria Knolls Slide, shifted about 32 cubic kilometres of sediment. That's more than 30 times the size of Uluru, the famous red monolith in Australia's Northern Territory. The landslide stretches for 20km along the coast, up to 8km wide and its depth ranges from 250m to more than 1km .

Fallout from the event is scattered over a wide area in the Queensland Trough, forming knolls more than 300m high and 3km long. They harbour both living and fossilised corals – including gorgonian sea whips, bamboo corals, molluscs and stalked barnacles – providing a clue to the age and origin of the knolls.

The Great Barrier ReefiStock

"We were amazed to discover this cluster of knolls while 3D-multibeam mapping the deep Great Barrier Reef seafloor," said study author Robin Beaman of James Cook University, Australia, in a statement.

"The oldest fossil corals recovered off the top of the knoll was 302,000 years old, which means the landslide event that caused these knolls must be older," said Angel Puga-Bernabéu of the University of Granada, Spain, also a study author.

North-westerly view of the Gloria Knolls Slide and Gloria Knolls. Depths are red (shallow) to blue (deep), over a depth range of about 1,700mwww.deepreef.org

In addition to the knolls, there are 70 smaller blocks of debris. This unusual underwater landscape was what prompted dredging and further investigation of the reef seafloor using 3D imaging.

"What we discovered was the smoking gun," Beaman told BBC News. "It was quite clear that those knolls were the remains of a very large undersea landslide that had occurred some time ago."

Westerly view of the Gloria Knolls. Depths are red (shallow) to blue (deep), over a range of about 1,500m.www.deepreef.org